Geochemical and isotopic indicators of hydrodynamic systems in crystalline rock mass

The regularities of groundwater movement in crystalline rock masses are considered. Multidimensional techniques are used to treat the hydrogeological and hydrogeochemical data collected in sites with different conditions of groundwater formation. Sets of informative indicators are chosen for the decomposition of hydrogeological systems. Approaches to assessing the information content of empiric data are proposed. © MAIK "Nauka/Interperiodica" 2002.

Авторы
Khaustov A.P. 1 , Grabar' A.V.2 , Lomonosov I.S.3 , Yanxin W.4
Редакторы
-
Журнал
Издательство
-
Номер выпуска
1
Язык
Английский
Страницы
33-42
Статус
Опубликовано
Подразделение
-
Номер
-
Том
29
Год
2002
Организации
  • 1 Peoples Friendship University, Podol'skoe shosse 8/5, Moscow 113093, Russian Federation
  • 2 Nedra Limited Society, ul. Krzhizhanovskogo 24/35, Moscow 117218, Russian Federation
  • 3 Institute of Geochemistry, Siberian Brabnch, Russian Academy of Sciences, ul. Favorskogo 1, Irkutsk 664033, Russian Federation
  • 4 Chinese Geological University, Uhan 430074, China
Ключевые слова
Crystalline rocks; Geochemistry; Groundwater; Hydrodynamics; Hydrogeology; Isotopes; crystalline rock; groundwater; hydrodynamics; hydrogeochemistry; isotopic composition; rock mass response
Дата создания
19.10.2018
Дата изменения
19.10.2018
Постоянная ссылка
https://repository.rudn.ru/ru/records/article/record/254/